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v zr
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     Determination of Be, Cr, Mo, V, Zr and Ge by microwave induced plasma atomic emission spectrometry was investigated.
     研究了用微波诱导等离子体原子发射光谱法(MIP-AES)测定Be、Cr、Mo、V、Zr和Ge。
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     The operating conditions were optimized. The detection limits for Be, Cr, Mo, V, Zr, and Ge were 0.038,0.030, 0.015,0.030,0.024 and 0.11μg/ml, respectively.
     确定了最佳实验条件,其检出限分别为:0.038,0.030,0.015,0.030,0.024和0.11μg/ml。
短句来源
     The results obtained are as follows: Amounts of elements Be, P, Pb, U, Ga, Sn, V, Zr, Ag, Y, Sr, Ba, Bi,Sb,Cd, W and In in diamonds are under the detection limits of spectral analysis.
     测试结果表明:Be、P、Pb、u、Ga、Sn、V、Zr、Ag、Y、Sr、Ba、Bi、Sb、Cd、W和In等元素在金刚石中的含量均在光谱分析的检测限以下。
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     A new ICP-AES procedure to determine the impurities in Pd-Ag alloys, such as Pb, Sb, Bi, As, Sn, In, Al, Fe, V, Zr, Cr, Be, Cu, Ni, Ca, Mg, Co, Pt, Ir, Au, Zn, and Cd, was developed. This method involves separating Pd and Ag from the impurities using coprecipitation with Y(OH)_3 and precipitating AgCl.
     采用氢氧化钇共沉淀及氯化银沉淀法将合金成份Pd、Ag与被测杂质元素分离,研究了Pd—Ag合金中Pb、Sb、Bi、As、Sn、In、Al、Fe、V、Zr、Cr、Be、Cu、Ni、Ca、Mg、Co、Pt、Ir、Au、Zn、Cd等22个杂质元素的ICP—AES测定方法。
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     The effects of Samarium contents and transition metal M (M=Co Cr V Zr) for Fe on the magnetic properties and thermal stabilities of Sm_2Fe_(17)N_x have been studied.
     过渡族元素(M=Co、Cr、V、Zr)部分取代铁对粉末压结体磁性能的影响和Sm_2Fe_(17)N_x化合物的稳定性。
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     Zr.
     Zr.
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     The ZR and the IAA contents were
     对于新红星苹果叶片内,ZR含量、IAA含量的显著增加分别发生在处理10小时后和6小时后,GA_3含量和ABA含量均在处理2小时后显著降低。
短句来源
     The experiments of W Zr binary system were evaluated.
     综合评估了W Zr体系的实验结果。
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     Investigation of the Intermetallic Precipitates in Zr-4
     Zr_(-4)合金中第二相的研究
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  v zr
2004-V ZR 267/03-, abrufbar unter www.bundesgerichtshof.de.zu Beweiserleichterungen Stellung zu den vorgeschlagenen L?sungsmodellen.
      
The convective velocity components vz' (r, z), vr' (r, z) and the temperature T are determined as functions of the cylindrical coordinates.
      
The results of the final fits for 1V-Nb and 1V-Zr are presented in Table 5.
      
Neither the 1V-Nb fit nor the 1V-Zr fit exceed the maximum number of free parameters.
      
For 1V-Zr, however, the Zr-O distance in the model was similar to the distance in ZrV2O7.
      


In the light of the quantitative analyses data of the trace elements contents in bauxite end clayof the Central-Western parts of Hcnan Province, the V/Zr, Sr/Ba, and B/Ga ratio curves were calculated. From these curves the complexities of the hydrodynamic condition. Palaeogeography and palaeogeomorphology during the metallogenic epoch are noted. It is believed that the bauxite is characterized by a multiphasic metallogenesis, and the bauxite deposits, being formed under a condition of abnormal seawater...

In the light of the quantitative analyses data of the trace elements contents in bauxite end clayof the Central-Western parts of Hcnan Province, the V/Zr, Sr/Ba, and B/Ga ratio curves were calculated. From these curves the complexities of the hydrodynamic condition. Palaeogeography and palaeogeomorphology during the metallogenic epoch are noted. It is believed that the bauxite is characterized by a multiphasic metallogenesis, and the bauxite deposits, being formed under a condition of abnormal seawater environment, belong to the multiple genesis type.

根据河南中西部铝土矿和粘土质岩石微量元素含量定量分析结果,以及由此而得出的V/Zr、Sr/Ba和B/Ga比值曲线,反映了成矿时水动力条件和古地理、古地貌的复杂性.认为铝土矿具有多阶段成矿的特点.矿床形成于非正常海水条件下,属多因复成矿床.

Both boninite and boni-basalt belong to the boninite series. They are enriched in large ion lithophilc elements (L1LE) and refractory elements but depleted in high field strength ions (HFSE) and HREE than MORB. In comparison to boni-basalts, boninites are rich in SiO2, LILE, Zr and Hf contents and low in Ti/Zr and V/Zr ratios but high in Zr/Y ratio- The REE patterns are characterized by LREE-enrichment and slight LREE-or MREE-depletion. Boni-basalts have higher Ti/Zr and V/Zr...

Both boninite and boni-basalt belong to the boninite series. They are enriched in large ion lithophilc elements (L1LE) and refractory elements but depleted in high field strength ions (HFSE) and HREE than MORB. In comparison to boni-basalts, boninites are rich in SiO2, LILE, Zr and Hf contents and low in Ti/Zr and V/Zr ratios but high in Zr/Y ratio- The REE patterns are characterized by LREE-enrichment and slight LREE-or MREE-depletion. Boni-basalts have higher Ti/Zr and V/Zr but lower Zr/Y ratios than those of the boninites. The REE distribution of boni-basalts is characterized by LREE-or MREE-depletion. There is little doubt that both boninites and boni-basalts were derived from primary magmas, but the significant differences in their geochemical composition suggest that they were originally derived from different sources. Boninites are confined to some locations in the West Pacific (e.g. Bonin, Mariana Trench, Cape Vogel in Papua New Guinea and New Calidonia), and only other two occurrences are known in Dingqin of China and Heathcote of Southeastern Australia. It seems possible that the boninites or low-Ti basalts recovered from ophiolites so far reported in the literature, with the exception of Dinqin and Heathcote, are almost corresponding to the boni-basalts, but do not represent true boninites, for example Troodos, Vourinos, Pindos, Betts Cove and Khan Taishir, as well as Xigaze in China. It is now generally accepted that the boninites in the West Pacific were formed in the fore-arc settings above the subduction zone, but the case may not be true for boni-basalts, which were formed in an initial back-arc basin environment during the early period of spreading of the back-arc basin-

玻安岩(boninite)和玻玄岩(bonibasalt)为玻安岩系的两个亚类。与大洋中脊玄武岩(MORB)相比,它们均富大离子亲石元素和亏损高场强元素。玻玄岩相对玻安岩略贫大离子亲石元素及Zr等,其CaO/Al_2O_3、Zr/Y、Ti/Zr及V/Zr值等均不同于玻安岩,二者系来自不同的源岩并产于不同的构造环境。玻玄岩通常产于弧后盆地扩张的初期阶段,而玻安岩则位于消减带之上的前弧环境。

Contents of 26 metal elements were determined for the commercial fishes from takes in Suzhou region. The results are as follows: 1) Magnitudes of contents of metal elements are in the order: benthic fishes>mid-waterfishes>upper-layer fishes, Fishes at higher levels in the food chain have higher contents than those at lower levels (i.e. carnivorous fishes> omnivorous fishes>herbivorous fishes). Contents in fish gills are higher than in the flesh. 2) The contents of metal elements are relatively stable in fishes...

Contents of 26 metal elements were determined for the commercial fishes from takes in Suzhou region. The results are as follows: 1) Magnitudes of contents of metal elements are in the order: benthic fishes>mid-waterfishes>upper-layer fishes, Fishes at higher levels in the food chain have higher contents than those at lower levels (i.e. carnivorous fishes> omnivorous fishes>herbivorous fishes). Contents in fish gills are higher than in the flesh. 2) The contents of metal elements are relatively stable in fishes from the same environment. There is a regional distribution of metal contents in fishes from polluted lakes. 3) The contents of metal elements in the freshwater fishes from the lakes in Suzhou region are not very high and are comparable to those in fishes from the Caspian Sea, U.S.S.R. The magnitudes of metal contents in fishes from Suzhou region are in the order:Fe>Zn>Sr>Cu>Pb>Ba>Li>Nb>Ga>Ni>Ce>Ti>Mn>Th>Co>Cr>As>Hg>Cd>V>Zr>Y>La>Be≥Yb>Mo.

1984—1985年,对苏州地区不同营养类型湖泊9种经济鱼类中26种金属元素含量进行了测定和分析。①在湖泊中污染区的鱼体金属元素含量要比非污染区高。②鱼对金属元素的吸收、富集规律是:底层鱼>中层鱼>上层鱼;食物链长的鱼>食物链短的鱼(即肉食性鱼>杂食性鱼>草食性鱼);鱼鳃>鱼肉。③在相同的环境条件和生长状况下,鱼体中金属元素含量具有相对的稳定性;鱼在污染性湖泊中具有区域性分布的特点,因而鱼也是污染物的指示者之一。④苏州地区湖泊鱼体中金属元素的自然含量不太高,与苏联里海地区的鱼类相近似;它们在鱼体内的排列次序为:铁>锌>锶>铜>铅>钡>锂>铌>镓>镍>铈>钛>锰>钍>钴>铬>砷>汞>镉>钒>锆>钇>镧>铍≥镱>钼。

 
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